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在确定出北加里曼丹大地构造单元的基础上,结合分析其内新生代岩浆岩性质及其大地构造环境,认为新生代北加里曼丹是卢卡尼亚(Luconia)陆块和巽他陆块碰撞的造山带,并提出“北加里曼丹新生代碰撞造山带”的概念。该造山带经历了边缘造山带-内部造山带-边缘造山带相继转化的过程,它控制了加里曼丹的区域成矿作用,特别是晚渐新世-中中新世北加里曼丹内部造山带的逆冲叠瓦阶段是加里曼丹区域成矿的最重要时期。
Based on the identification of the tectonic units of North Kalimantan and the analysis of the Meso-Cenozoic magmatic rocks and their tectonic setting, the Cenozoic North Kalimantan is considered to be Luconia landlock and Hallucock Block collision orogenic belt and proposed the concept of “North Kalimantan Cenozoic collision orogenic belt.” The orogenic belt undergoes the successive transformation of the marginal orogenic belt-the interior orogenic belt-the marginal orogenic belt, which controls the regional mineralization in Kalimantan, especially the Late Oligocene-Mid Miocentre Northern Kalimantan orogen The thrusting and shoaling phase of the belt is the most important period for metallogenesis in the Kalimantan region.